VPD.to.rH {bigleaf} | R Documentation |
Conversions between Humidity Measures
Description
Conversion between vapor pressure (e), vapor pressure deficit (VPD), specific humidity (q), and relative humidity (rH).
Usage
VPD.to.rH(
VPD,
Tair,
Esat.formula = c("Sonntag_1990", "Alduchov_1996", "Allen_1998"),
constants = bigleaf.constants()
)
rH.to.VPD(
rH,
Tair,
Esat.formula = c("Sonntag_1990", "Alduchov_1996", "Allen_1998"),
constants = bigleaf.constants()
)
e.to.rH(
e,
Tair,
Esat.formula = c("Sonntag_1990", "Alduchov_1996", "Allen_1998"),
constants = bigleaf.constants()
)
VPD.to.e(
VPD,
Tair,
Esat.formula = c("Sonntag_1990", "Alduchov_1996", "Allen_1998"),
constants = bigleaf.constants()
)
e.to.VPD(
e,
Tair,
Esat.formula = c("Sonntag_1990", "Alduchov_1996", "Allen_1998"),
constants = bigleaf.constants()
)
e.to.q(e, pressure, constants = bigleaf.constants())
q.to.e(q, pressure, constants = bigleaf.constants())
q.to.VPD(
q,
Tair,
pressure,
Esat.formula = c("Sonntag_1990", "Alduchov_1996", "Allen_1998"),
constants = bigleaf.constants()
)
VPD.to.q(
VPD,
Tair,
pressure,
Esat.formula = c("Sonntag_1990", "Alduchov_1996", "Allen_1998"),
constants = bigleaf.constants()
)
Arguments
VPD |
Vapor pressure deficit (kPa) |
Tair |
Air temperature (deg C) |
Esat.formula |
Optional: formula to be used for the calculation of esat and the slope of esat.
One of |
constants |
eps - ratio of the molecular weight of water vapor to dry air (-) |
rH |
Relative humidity (-) |
e |
Vapor pressure (kPa) |
pressure |
Atmospheric pressure (kPa) |
q |
Specific humidity (kg kg-1) |
References
Foken, T, 2008: Micrometeorology. Springer, Berlin, Germany.
[Package bigleaf version 0.8.2 Index]